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溜河地区为夹皮沟金矿集中区的组成部分之一。通过对溜河地区金矿成矿类型、控矿条件、成矿物质来源、成矿时代等特征的分析,对该区金矿成矿规律进行了初步探讨,认为溜河地区属于高级变质区,其成矿特征与夹皮沟花岗—绿岩带不同,该区金矿成矿应与北西向、近东西向脆-韧性剪切带以及中生代构造岩浆活动关系密切,对该区的下一步找矿具有指示意义。
The slippery river area is one of the components of the Jiapigou gold mine. Based on the analysis of ore-forming types, ore-controlling conditions, sources of metallogenic materials and metallogenic epoch of the gold deposits in the area of Liupo River, the metallogenic regularity of the gold deposits in the area is preliminarily discussed. It is believed that the area belongs to the advanced metamorphic area, Its mineralization is different from that of the Jiapigou granite-greenstone belt. The gold mineralization in this area should be closely related to the NW-trending, near-east-west brittle-ductile shear zone and the Mesozoic tectonic magmatism. For the next step in this area Prospecting has instructive significance.